In addition to the pressure balance given in Equation 7-73 and consideration for mass flux across the interface in
Equation 7-74 and
Equation 7-75, the Beavers–Joseph slip condition models the development of the boundary layer at the intersection of the physics interfaces using a small interface slip velocity.
Here, tr() is the trace operator, κ is the permeability tensor of the porous media,
v is the thin-film velocity, subscripts
b and
w represent the base and wall boundaries of the thin-film region, respectively, and the subscript
t represents the component tangential to the interface.